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Paleozoic large igneous provinces of Northern Eurasia: Correlation with mass extinction events

机译:欧亚大陆北部的古生代大火成岩省:与大规模灭绝事件的相关性

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摘要

This paper assesses data from recently described major Paleozoic large igneous provinces (LIPs), mostly in Northern Eurasia. The 10 LIPs reviewed form a unimodal distribution in terms of volume. Eight LIPs have an initial modal volume greater than 0.1 × 10~6 km~3. The rift associated basalts of 2 LIPs from the end of the Late Cambrian Period and the end of the Late Ordovician Period do not occupy a large volume. Some of the provinces were discovered or rediscovered relatively recently and dating is still approximate, but most provinces fit a simple model in which volcanism persisted on the order of 10-20 Myr, often resulting in continental break-up. Correlation between LIP ages and the ages of geological events in the Paleozoic Era that reflect mass extinctions and oceanic anoxia agrees with correlations suggested by Courtillot (1994) and Courtillot and Renne (2003) for the Cenozoic and Mesozoic eras, considering that the absolute dating of some Paleozoic LIPs needs to be strengthened in the future.
机译:本文评估了最近描述的主要古生代大火成岩省(LIP)的数据,这些省大多位于北欧亚大陆。审查的10个LIP在数量上形成了单峰分布。八个LIP的初始模态体积大于0.1×10〜6 km〜3。从寒武纪末期到奥陶纪末期,两个裂谷的裂谷相关玄武岩所占比例不大。一些省份是在相对较新的时期发现或重新发现的,其年代仍然是近似的,但是大多数省份都采用了一种简单的模型,在该模型中,火山活动持续在10-20 Myr的数量级,常常导致大陆破裂。 LIP年龄与反映大规模灭绝和海洋缺氧的古生代地质事件年龄之间的相关性与Courtillot(1994)和Courtillot和Renne(2003)提出的有关新生代和中生代的相关性一致。将来需要加强一些古生界的LIP。

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